26 research outputs found
Reviewing evidence of marine ecosystem change off South Africa
Recent changes have been observed in South African marine ecosystems. The main pressures on these
ecosystems are fishing, climate change, pollution, ocean acidification and mining. The best long-term datasets are
for trends in fishing pressures but there are many gaps, especially for non-commercial species. Fishing pressures
have varied over time, depending on the species being caught. Little information exists for trends in other
anthropogenic pressures. Field observations of environmental variables are limited in time and space. Remotely
sensed satellite data have improved spatial and temporal coverage but the time-series are still too short to
distinguish long-term trends from interannual and decadal variability. There are indications of recent cooling on the
West and South coasts and warming on the East Coast over a period of 20 - 30 years. Oxygen concentrations on the
West Coast have decreased over this period. Observed changes in offshore marine communities include southward
and eastward changes in species distributions, changes in abundance of species, and probable alterations in
foodweb dynamics. Causes of observed changes are difficult to attribute. Full understanding of marine ecosystem
change requires ongoing and effective data collection, management and archiving, and coordination in carrying out
ecosystem research.DHE
Life strategies, energetics and growth characteristics of Calanoides carinatus (Copepoda) in the Angola-Benguela frontal region
Rates of daily egg production, moulting and egg hatching success, as well as total lipid content and composition of Calanoides carinatus, were measured in the region of the southern Angola Current (SAC), the Angola-Benguela Front (ABF) and the coastal upwelling area of the northern Benguela Current (NBC) system during February–March 2002. There were distinct differences in the vertical distribution, growth characteristics, lipid content and composition of populations in the SAC/ABF and NBC regions, indicative of different physiological states. Whereas in the NBC, C. carinatus was actively growing in response to elevated chlorophyll a levels associated with coastal upwelling, it comprised deep-living C5 copepodids with very large wax ester reserves (c. 40–50% dry mass) and extremely low metabolism in the SAC/ABF, suggesting diapause. This study provides the first data on lipid composition (lipid classes, fatty acids and alcohols) of this copepod in the region; in particular, the diapausing C5s contained high levels of long-chain, mono-unsaturated fatty acids (23% of all fatty acids) and alcohols (69% of all fatty alcohols) in addition to trophic markers of diatoms, viz. 16:1(n-7) and 20:5(n-3). Based on total lipid content, the maximum survival time of the diapausal component of C. carinatus was estimated to be 149–192 days, whereas active surface-dwelling C5s and females could not survive for more than 10 days without feeding.Keywords: Angola-Benguela Front, Calanoides carinatus, diapause, growth rates, lipid content and composition, northern Benguela upwelling, oxygen minimum layer, vertical distribution African Journal of Marine Science 2005, 27(3): 641–65
Analysis of 1Â year virtual histology changes in coronary plaque located behind the struts of the everolimus eluting bioresorbable vascular scaffold
Serial intravascular ultrasound virtual histology (IVUS-VH) after implantation of metallic stents has been unable to show any changes in the composition of the scaffolded plaque overtime. The everolimus-eluting ABSORB scaffold potentially allows for the formation of new fibrotic tissue on the scaffolded coronary plaque during bioresorption. We examined the 12Â month IVUS-VH changes in composition of the plaque behind the struts (PBS) following the implantation of the ABSORB scaffold. Using IVUS-VH and dedicated software, the composition of the PBS was analyzed in all patients from the ABSORB Cohort B2 trial, who were imaged with a commercially available IVUS-VH console (s5i system, Volcano Corporation, Rancho Cordova, CA, USA), immediately p